a.b. viirs backscattering @551nm (nov. 20, 2013)
TRANSCRIPT
A. B. VIIRS Backscattering @551nm (Nov. 20, 2013)
GEOCAPE / Northern Gulf of Mexico Cruise July 9-19, 2013 - Scatter
Slope rrs412 rrs443 rrs488 rrs547 rrs667MODIS 0.85 0.82 0.94 1.07 1.18
VIIRS v01 0.5 0.72 0.85 0.91 0.79VIIRS v02 0.79 0.91 0.97 0.99 0.85
Rsquared rrs412 rrs443 rrs488 rrs547 rrs667MODIS 0.91 0.86 0.85 0.86 0.92
VIIRS v01 0.44 0.77 0.89 0.92 0.91VIIRS v02 0.40 0.78 0.88 0.92 0.91
Insitu: UMASS/NOAA
A. B.
C.D.
1:1 Line
VIIRS1815 GMT
Bb_551_qaa
Rrs Stations – Handheld RadiometerFlowthru Stations – AC9
A
B
MODIS & VIIRSVery Similar!
VIIRS1815 GMT
Bb_551_qaa
Flowthru Stations – AC9
SLOPE a412 a443 a488 a547 c412 c443 c488 c547MODQAA 1.48 1.38 1.15 0.88 1.41 1.43 1.43 1.43VIIRSQAA 0.85 1.05 0.99 0.83 1.37 1.47 1.48 1.47
R2 a412 a443 a488 a547 c412 c443 c488 c547ModQAA 0.90 0.91 0.91 0.84 0.59 0.59 0.58 0.58VIIRS QAA 0.80 0.90 0.88 0.79 0.71 0.72 0.70 0.70
19 Stations
A. MODIS (1855 GMT) ALMS
LA
FL
B. SNPP VIIRS (1925 GMT) ALMS
LA
FL
0.5
0.13
0.032
0.0079
0.002
0.0005
m-1
GEOCAPE / Northern Gulf of Mexico Cruise September 9-19, 2013 Rrs and IOP Station Locations
Insitu: UMASS/NOAA
VIIRS Mean Backscattering @551nm (September 9-19, 2013)
GEOCAPE / Northern Gulf of Mexico Cruise July 9-19, 2013 - Spectral
Insitu: UMASS/NOAA
Insitu: UMASS (Lee) & NOAA (Ondrusek) 25 Valid Matchups
Slope rrs412 rrs443 rrs488 rrs547 rrs667MODIS 0.85 0.82 0.94 1.07 1.18
VIIRS v01 0.5 0.72 0.85 0.91 0.79VIIRS v02 0.79 0.91 0.97 0.99 0.85
Rsquared rrs412 rrs443 rrs488 rrs547 rrs667MODIS 0.9852 0.9800 0.9692 0.9713 0.9720
VIIRS v01 0.9059 0.9668 0.9841 0.9826 0.9582VIIRS v02 0.8768 0.9638 0.9801 0.9788 0.9573
Insitu: UMASS (Lee) & NOAA (Ondrusek)
SLOPE a412 a443 a488 a547 c412 c443 c488 c547ModQAA 1.24 1.30 1.08 0.99 1.41 1.51 1.52 1.54VIIRS QAA 1.21 1.32 1.00 0.89 1.11 1.27 1.32 1.33
R2 a412 a443 a488 a547 c412 c443 c488 c547ModQAA 0.93 0.96 0.95 0.97 0.95 0.96 0.96 0.97VIIRS QAA 0.93 0.88 0.96 0.97 0.92 0.93 0.92 0.93
A. B.
C. D.
GEOCAPE / Northern Gulf of Mexico Cruise July 9-19, 2013 - Scatter
SLOPE a412 a443 a488 a547 c412 c443 c488 c547ModLMI 1.27 1.28 1.45 1.56 1.56 1.82 2.22 2.69ModQAA 1.24 1.30 1.08 0.99 1.41 1.51 1.52 1.54VIIRS LMI 1.42 1.66 1.40 1.51 1.33 1.71 2.07 2.59VIIRS QAA 1.21 1.32 1.00 0.89 1.11 1.27 1.32 1.33
R2 a412 a443 a488 a547 c412 c443 c488 c547ModLMI 0.01 0.02 0.05 0.06 0.91 0.92 0.94 0.95ModQAA 0.20 0.78 0.75 0.99 0.92 0.93 0.93 0.93VIIRS LMI 0.75 0.68 0.68 0.55 0.88 0.88 0.85 0.85VIIRS QAA 0.79 0.73 0.87 0.87 0.86 0.88 0.87 0.87
Insitu: UMASS/NOAA
GEOCAPE / Northern Gulf of Mexico Cruise July 9-19, 2013 - Spectral
NOAA ECOPUC Data(Ondrusek)
bb440 Rsquared Slopemodis qaa 0.9895 0.5600viirs qaa 0.9586 0.7500vocco 0.8408 1.1300
RV Ocean Color Cruise – November 20, 2013 – Mississippi SoundRrs and IOP (Surface FlowThru +/- 30 Minutes from Satellites)
VIIRS1815 GMT
Bb_551_qaa
Rrs Stations – Handheld RadiometerFlowthru Stations – AC9
VIIRS
Comparison Between MODIS and VIIRS - November 20, 2013Mississippi Sound
QAA Total Backscattering (551nm for VIIRS & 547nm for MODIS Aqua)
MODIS Aqua
Biloxi, MSBay St. Lous, MS
Slidell, LA
Biloxi, MSBay St. Lous, MS
Slidell, LA
A. B.
C. D.
1:1 1:1
1:1Slope rrs443 rrs488 rrs547
MODIS 1845 1.09 0.97 0.95VIIRS 1957 0.83 0.89 1.06
Rsquared rrs443 rrs488 rrs547MODIS 1845 0.94 0.93 0.81VIIRS 1957 0.92 0.94 0.87
A. B.
C. D.
R/V Ocean Color Cruise Mississippi Sound November 20, 2013 FlowThru (+/- 30 minutes of early/late satellite pass)
MODIS & VIIRSVery Similar!
Satellite bb/b Insitu profile bb/b0.018616497 0.018218296
19 Stations
SLOPE a412 a443 a488 a547 c412 c443 c488 c547ModQAA 1.4719 1.3683 1.1459 0.8762 1.3836 1.4048 1.4270 1.4263VIIRS QAA 0.8398 1.0374 0.9853 0.8244 1.3357 1.4410 1.4748 1.4678
R2 a412 a443 a488 a547 c412 c443 c488 c547ModQAA 0.9968 0.9966 0.9961 0.9974 0.9875 0.9872 0.9871 0.9873VIIRS QAA 0.9929 0.9966 0.9958 0.9965 0.9915 0.9914 0.9908 0.9909
R/V Ocean Color Cruise Mississippi Sound November 20, 2013 FlowThru (+/- 30 minutes of early/late satellite pass)
SLOPE a412 a443 a488 a547ModLMI 1.95 2.03 1.96 1.73ModQAA 1.48 1.38 1.15 0.88VIIRS LMI 0.93 1.22 1.46 1.56VIIRS QAA 0.85 1.05 0.99 0.83
R2 a412 a443 a488 a547ModLMI 0.86 0.88 0.89 0.84ModQAA 0.90 0.91 0.91 0.84VIIRS LMI 0.72 0.78 0.84 0.78VIIRS QAA 0.80 0.90 0.88 0.79
R/V Ocean Color Cruise Mississippi Sound November 20, 2013 FlowThru (+/- 30 minutes of early/late satellite pass)
SLOPE a412 a443 a488 a547ModLMI 1.95 2.03 1.96 1.73ModQAA 1.48 1.38 1.15 0.88VIIRS LMI 0.93 1.22 1.46 1.56VIIRS QAA 0.85 1.05 0.99 0.83
R2 a412 a443 a488 a547ModLMI 0.86 0.88 0.89 0.84ModQAA 0.90 0.91 0.91 0.84VIIRS LMI 0.72 0.78 0.84 0.78VIIRS QAA 0.80 0.90 0.88 0.79
c412 c443 c488 c5471.84 2.09 2.45 2.841.41 1.43 1.43 1.431.56 1.89 2.24 2.751.37 1.47 1.48 1.47
c412 c443 c488 c5470.31 0.27 0.22 0.180.59 0.59 0.58 0.580.67 0.69 0.68 0.660.71 0.72 0.70 0.70
MODIS & VIIRSVery Similar!
Evaluation of GOCI, MODIS, and VIIRS ImageryObjective
• Evaluate current NRL processing of GOCI level 1b water leaving radiance (nLw)
• Provide an inter-sensor comparison between GOCI, MODIS, and VIIRS remote sensing reflectances
• Compare GOCI, MODIS, and VIIRS with East China Sea Aeronet Ocean Color (Gageocho and Ieodo) data
22Session 42 Optical Remote Sensing
2014 AGU OCEAN SCIENCES (Crout, et.al.)
Evaluation of GOCI, MODIS, and VIIRS ImageryBackground - Data
• MODIS– Processed with MOBY gains
• VIIRS– Processed with MOBY gains
• GOCI– Processed with MODIS-SWIR-derived vicarious calibration gains– GOCI data from 4Z GTM (corresponds to local 1 pm)
• Reduces sun glint and sensor issues
• Aeronet SeaPrism– Gageocho Aeronet (SeaPrism #624) was moved to Ieodo
• Results in a data gap from May 2012 – December 2013• The quality control of the data is near real time?
23Session 42 Optical Remote Sensing
Evaluation of GOCI, MODIS, and VIIRS ImageryBackground - Processing
• Operational Ocean Color Processing– NRL’s Automated Processing System (APS) based on n2gen
software (NRL/NASA R&D)– Level 1b data obtained from NOAA CLASS (MODIS) and
NAVO (GOCI and MODIS)– Atmospheric correction using Gordon-Wang NIR with 80
aerosol models– Glint and cloud removal
24Session 42 Optical Remote Sensing
Session 42 Optical Remote Sensing 25
Evaluation of GOCI, MODIS, and VIIRS Imagery
JD 118 2012 Spectra – Gageocho and Ieodo
rrs_412 rrs_443 rrs_490 rrs_555 rrs_660
-0.002
1.73472347597681E-18
0.002
0.004
0.006
0.008
0.01
GOCI Gains (G)
GOCI no Gains
GOCI Gains (I)
GOCI no Gains (I)
VIIRS Gains (G)
VIIRS no Gains (G)
VIIRS Gains (I)
VIIRS no Gains (I)
In situ (G)
MODIS (G)
MODIS (I)
Ieodo
Gageocho
Session 42 Optical Remote Sensing 26
Evaluation of GOCI, MODIS, and VIIRS Imagery
JD 277 2013 Spectra – Gageocho
rrs_412 rrs_443 rrs_490 rrs_555 rrs_660
-0.002
1.73472347597681E-18
0.002
0.004
0.006
0.008
0.01
GOCI GainsGOCI no GainsVIIRS GainsVIIRS no GainsMODIS (G)
Session 42 Optical Remote Sensing 27
rrs_412 rrs_443 rrs_490 rrs_555 rrs_6600
0.002
0.004
0.006
0.008
0.01
0.012
0.014
0.016
0.018
0.02
GOCI Gains (I)GOCI no Gains (I)VIIRS Gains (I)VIIRS no Gains (I)In situ (i)MODIS (I)
Evaluation of GOCI, MODIS, and VIIRS Imagery
JD 341 2013 spectra – Ieodo
Session 42 Optical Remote Sensing 28
Evaluation of GOCI, MODIS, and VIIRS Imagery
All sensors (4Z) time series - rrs 550
JD 108 JD 117 JD 118 G JD 118 I JD 124 JD 138 JD 277 JD 341 G JD 341 I JD 346 0
0.005
0.01
0.015
0.02
0.025
In situMODISGOCIVIIRS
Session 42 Optical Remote Sensing 29
Evaluation of GOCI, MODIS, and VIIRS Imagery - bb 551nm
JD 277 ImageryGOCI No Gains MODIS
VIIRSGains
GOCIGains
VIIRS No Gains
bad
Session 42 Optical Remote Sensing 30
Evaluation of GOCI, MODIS, and VIIRS Imagery
JD 277 Full Image comparison to sites from multiple images - R2 Values
R2 Values Multiple Images, Single Sample Single Image, all samples
Channel GOCI-MODIS VIIRS-MODIS GOCI-MODIS VIIRS-MODIS
412 0.539 0.970 0.842 0.942
443 0.835 0.993 0.943 0.971
490 0.930 0.992 0.976 0.985
555 0.980 0.979 0.983 0.990
690 0.959 0.914 0.972 0.983
Compared to MODIS, VIIRS doing a little better overall than GOCI (mainly 412).All three sensors consistent.
Session 42 Optical Remote Sensing 31
Evaluation of GOCI, MODIS, and VIIRS Imagery
Conclusions
• MODIS, VIIRS, and GOCI remote sensing reflectances compare favorably in the East China Sea
• Application of Gains to GOCI and VIIRS visibly improves data
• Application of Gains lowers rrs in most cases– GOCI 412 and 443 channels appear to be exceptions
• Data from single points and imagery show similar statistics, except at GOCI 412 and 443 Channels
• Overall, the comparison between the sensors are good